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Growth of subcontinental lithospheric mantle beneath Zimbabwe started at or before 3.8 Ga: Re-Os study on chromites
Th F. Nägler
*
, J. D. Kramers, B. S. Kamber,
R. Frei
, M. D.A. Prendergast
*
Corresponding author for this work
Geology
59
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Earth & Environmental Sciences
chromite
100%
mantle
64%
Archean
54%
craton
27%
forward modeling
16%
Southern Africa
15%
xenolith
15%
silicate
12%
isotope
10%